Kimrobinsonite is a very rare tantalum hydroxide mineral typically found as small, cubic crystals within highly evolved granitic pegmatites. It is primarily identified through chemical analysis due to its scarcity and similarity to other members of the pyrochlore supergroup.
Is this kimrobinsonite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch kimrobinsonite with a known reference. Kimrobinsonite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kimrobinsonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Kimrobinsonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: cubic. Typical habit: equant crystals.
Often found alongside kimrobinsonite
Minerals reported to co-occur with kimrobinsonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ta(OH)₅
- Mohs hardness
- 2.5
- Density
- 4.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Equant Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Granite Pegmatites
- Typical price
- $200-1000+ per specimen
Where rockhounds find kimrobinsonite
Classic worldwide localities
- Kola Peninsula, Russia
Field-hunting tip
Look in granite pegmatites country — that is the host setting where kimrobinsonite typically forms. If you start seeing kesterite, stannite, quartz in float, you are in the right ground. Field specimens usually show a equant crystals habit, so train your eye for that shape before scanning the outcrop.


